Grassland soil

Fig. 11-12 Detrital carbon dynamics for the 0-20 cm layer of chernozem grassland soil. Carbon pools (kg C/ m ) and annual transfers (kg C/m per year) are indicated. Total profile content down to 20 cm is 10.4 kg C/m. (Reproduced with permission from W. H. Schlesinger (1977). Carbon balance in terrestrial detritus, Ann. Rev. Ecol. Syst. 8,51-81, Annual Reviews, Inc.)...

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Bunzl K, Forster H, Kracke W, et al. 1994. Residence times of fallout 239l240Pu, 238Pu,241 Am and 137Cs in the upper horizons of an undisturbed grassland soil. J Environ Radioact 22 11-27. 

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RYDEN, J.C., LOCKYER, D.R. and BRISTOW, A.W. (1983). Circulation of mineral elements within the environment of forage plants. Gaseous nitrogen losses from grassland soils. Annual Report 1982, 25-32, Hurley, The Grassland Research Institute. 

Namdeo, K.N. Persistence of dalapon in grassland soil. Plant and Soil, 31 445-448, 1972. 

Scifres, D.J. and Allen, TJ. Dissipation of dicamba from grassland soils of Texas, Weed Sci., 21 393-396, 1973. 

McGrath, D. (1997) Extractability, chemical composition, and reactivities of soil organic matter of Irish grassland soils. In Hayes, M.H.B. and Wilson, W.S. (eds) hfumic Substances in Soils, Peats and Waters. The Royal Society of Chemistry, Cambridge, UK, pp. 31-38. 

Turner, B.L. and Haygarth, P.M. (2000) Phosphorus forms and concentrations in leachate under four grassland soil types. Soil Science Society of America Journal 64(3), 1090-1099. 

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